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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >The build up of the isotopic signal in skeletons of the stony coral Porites lutea
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The build up of the isotopic signal in skeletons of the stony coral Porites lutea

机译:石质珊瑚Porites lutea骨骼中同位素信号的建立

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摘要

The build up of the isotopic signal in corals was followed by sampling the newly formed skeleton at a monthly resolution for a period of two years in order to establish the interrelations between the calcification processes and the skeletal isotopic composition. We deployed two underwater sampling schemes, which provide a monitor of the changes in water temperature and δ~(18)O and in the corresponding newly accreted skeleton of undisturbed Porites lutea colonies under natural conditions and four transplanted colonies, which maintained the genetic identity throughout the experiment. The results indicate that δ~(18)O of the newly accreted skeleton does not correlate with ambient temperature although the seasonal temperature variability at the site (winter to summer) is in the order of 6°C and δ~(18)O of seawater is constant throughout the year. In contrast to the newly formed surface skeleton, the isotopic compositions of the deep and older parts of the skeleton show the predicted annual isotopic pattern with highly significant correlation between δ~(18)O_s and SST. The transformation between temperature-independent to temperature-dependent isotopic signal occurs several months after the skeleton was formed at the surface. The position of the skeleton in relation to the open sea may generate the difference between δ~(18)O_s of the surface skeleton and that of the skeleton previously accreted further down the tissue layer. Our data support the general model of a multi-step skeletogenesis process, where the temperature independent skeleton is entails the first step, the production of skeletal scaffold, and the environmental temperature signature is captured by the next two other steps: the thickening and the periodic abrupt uplift occurring at the depth of the tissue layer. However, re-examination and development of the current isotopic models for coral calcification are required in order to explain the observed different temperature dependency during the growth's sequence.
机译:在珊瑚中建立同位素信号后,以每月分辨率对新形成的骨骼进行采样,为期两年,以建立钙化过程与骨骼同位素组成之间的相互关系。我们采用了两种水下采样方案,它们可以监测水温和δ〜(18)O的变化,以及在自然条件下未受干扰的Porites lutea菌落和四个移植菌落的相应新分泌骨骼中的变化,这些菌落始终保持了遗传特性。本实验。结果表明,尽管该部位(冬至夏季)的季节温度变化约为6℃,而新近生长的骨骼的δ〜(18)O约为6°C,但其与环境温度无关。全年的海水保持恒定。与新形成的表面骨架相反,骨架深部和较老部分的同位素组成显示出预测的年度同位素模式,在δ〜(18)O_s与SST之间具有高度显着的相关性。温度无关同位素信号到温度依赖性同位素信号之间的转换发生在骨架在表面形成数月后。骨骼相对于公海的位置可能会在表面骨骼的δ〜(18)O_s与先前在组织层下方逐渐积聚的骨骼的δ〜(18)O_s之间产生差异。我们的数据支持多步骤骨骼生成过程的一般模型,其中第一步是与温度无关的骨架,第二步是骨架支架的生产,随后两个步骤捕获环境温度特征:增厚和周期性在组织层的深度突然隆起。但是,需要重新检查和开发当前用于珊瑚钙化的同位素模型,以便解释在生长过程中观察到的不同温度依赖性。

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